Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)

Artificial river diversions cause intense and unpredictable changes in the geomorphological evolution and sedimentary dynamics of deltas. This study analyzes the effects of the 1958 course diversion of the Turbo River delta, Gulf of Urabá, southern Caribbean Sea. Recent satellite images were analyze...

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Autores:
Alcantara-Carrio, Javier
Caicedo, Ana
C. Hernandez, Jonny
Jaramillo-Velez, Alfredo
P. Manzolli, Rogerio
Tipo de recurso:
Article of journal
Fecha de publicación:
2019
Institución:
Corporación Universidad de la Costa
Repositorio:
REDICUC - Repositorio CUC
Idioma:
eng
OAI Identifier:
oai:repositorio.cuc.edu.co:11323/2840
Acceso en línea:
https://hdl.handle.net/11323/2840
https://doi.org/10.2112/JCOASTRES-D-17-00221.1
https://repositorio.cuc.edu.co/
Palabra clave:
Delta evolution
river diversion
spit
sand barrier
beach
ENSO
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openAccess
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id RCUC2_0e4b7b52910a28ca3304a58e5e79b515
oai_identifier_str oai:repositorio.cuc.edu.co:11323/2840
network_acronym_str RCUC2
network_name_str REDICUC - Repositorio CUC
repository_id_str
dc.title.spa.fl_str_mv Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
title Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
spellingShingle Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
Delta evolution
river diversion
spit
sand barrier
beach
ENSO
title_short Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
title_full Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
title_fullStr Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
title_full_unstemmed Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
title_sort Sediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)
dc.creator.fl_str_mv Alcantara-Carrio, Javier
Caicedo, Ana
C. Hernandez, Jonny
Jaramillo-Velez, Alfredo
P. Manzolli, Rogerio
dc.contributor.author.spa.fl_str_mv Alcantara-Carrio, Javier
Caicedo, Ana
C. Hernandez, Jonny
Jaramillo-Velez, Alfredo
P. Manzolli, Rogerio
dc.subject.spa.fl_str_mv Delta evolution
river diversion
spit
sand barrier
beach
ENSO
topic Delta evolution
river diversion
spit
sand barrier
beach
ENSO
description Artificial river diversions cause intense and unpredictable changes in the geomorphological evolution and sedimentary dynamics of deltas. This study analyzes the effects of the 1958 course diversion of the Turbo River delta, Gulf of Urabá, southern Caribbean Sea. Recent satellite images were analyzed and beach topography was monitored to obtain the shoreline migration and sediment budget; surface sediments were seasonally sampled, and their grain size parameters were determined; and seasonal sediment transport directions were deduced according to grain size trends. It was concluded that the bimodal wave regime controls the seasonal sedimentary patterns associated with southward longshore transport during both the dry and rainy seasons, and the northward longshore transport occurs in the midsummer drought. Beach morphodynamics of Yarumal Point, close to the present-day river mouth, show that this is the most exposed sector to waves, whereas fluvial sediment inputs are evidenced by a decrease in mean grain size and by poorly sorted sediments in the rainy season. A new spit is forming in Yarumal Point, with an intense increase in area and a westward progradation related to high fluvial sediment inputs from the La Niña event of 2010–12 and low erosion from the El Niño events of 2009–10 and 2015–16. In the central sector, longshore drift has formed the Yarumal barrier spit with a southeastward progradation that recently closed the interdistributary El Uno Bay. Consequently, a humaninduced sand barrier–lagoon system resulted with a stable or slightly regressive shoreline. Moreover, the Yarumal barrier spit has generated a new sediment bypass to Barajas Beach in the northern limit of the Las Vacas spit (i.e. the ancient delta lobe). Therefore, there is an unusual accretion of the abandoned delta lobe by sediment supply from the new lobe.
publishDate 2019
dc.date.accessioned.none.fl_str_mv 2019-03-07T20:25:40Z
dc.date.available.none.fl_str_mv 2019-03-07T20:25:40Z
dc.date.issued.none.fl_str_mv 2019-01
dc.type.spa.fl_str_mv Artículo de revista
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_6501
dc.type.content.spa.fl_str_mv Text
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
dc.type.redcol.spa.fl_str_mv http://purl.org/redcol/resource_type/ART
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/acceptedVersion
format http://purl.org/coar/resource_type/c_6501
status_str acceptedVersion
dc.identifier.issn.spa.fl_str_mv 1551-5036
dc.identifier.uri.spa.fl_str_mv https://hdl.handle.net/11323/2840
dc.identifier.doi.spa.fl_str_mv https://doi.org/10.2112/JCOASTRES-D-17-00221.1
dc.identifier.instname.spa.fl_str_mv Corporación Universidad de la Costa
dc.identifier.reponame.spa.fl_str_mv REDICUC - Repositorio CUC
dc.identifier.repourl.spa.fl_str_mv https://repositorio.cuc.edu.co/
identifier_str_mv 1551-5036
Corporación Universidad de la Costa
REDICUC - Repositorio CUC
url https://hdl.handle.net/11323/2840
https://doi.org/10.2112/JCOASTRES-D-17-00221.1
https://repositorio.cuc.edu.co/
dc.language.iso.none.fl_str_mv eng
language eng
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spelling Alcantara-Carrio, JavierCaicedo, AnaC. Hernandez, JonnyJaramillo-Velez, AlfredoP. Manzolli, Rogerio2019-03-07T20:25:40Z2019-03-07T20:25:40Z2019-011551-5036https://hdl.handle.net/11323/2840https://doi.org/10.2112/JCOASTRES-D-17-00221.1Corporación Universidad de la CostaREDICUC - Repositorio CUChttps://repositorio.cuc.edu.co/Artificial river diversions cause intense and unpredictable changes in the geomorphological evolution and sedimentary dynamics of deltas. This study analyzes the effects of the 1958 course diversion of the Turbo River delta, Gulf of Urabá, southern Caribbean Sea. Recent satellite images were analyzed and beach topography was monitored to obtain the shoreline migration and sediment budget; surface sediments were seasonally sampled, and their grain size parameters were determined; and seasonal sediment transport directions were deduced according to grain size trends. It was concluded that the bimodal wave regime controls the seasonal sedimentary patterns associated with southward longshore transport during both the dry and rainy seasons, and the northward longshore transport occurs in the midsummer drought. Beach morphodynamics of Yarumal Point, close to the present-day river mouth, show that this is the most exposed sector to waves, whereas fluvial sediment inputs are evidenced by a decrease in mean grain size and by poorly sorted sediments in the rainy season. A new spit is forming in Yarumal Point, with an intense increase in area and a westward progradation related to high fluvial sediment inputs from the La Niña event of 2010–12 and low erosion from the El Niño events of 2009–10 and 2015–16. In the central sector, longshore drift has formed the Yarumal barrier spit with a southeastward progradation that recently closed the interdistributary El Uno Bay. Consequently, a humaninduced sand barrier–lagoon system resulted with a stable or slightly regressive shoreline. Moreover, the Yarumal barrier spit has generated a new sediment bypass to Barajas Beach in the northern limit of the Las Vacas spit (i.e. the ancient delta lobe). Therefore, there is an unusual accretion of the abandoned delta lobe by sediment supply from the new lobe.Alcantara-Carrio, Javier-4196828f-b684-4972-8c52-c626dd383519-0Caicedo, Ana-382e7dde-9bd7-4d84-9821-842884e057e8-0C. Hernandez, Jonny-072a1fd7-3a17-451c-bed0-e75eccd76ccc-0Jaramillo-Velez, Alfredo-bcf41fc7-403a-4cb3-a6d7-50d53f7785ff-0P. Manzolli, Rogerio-0fa01e2a-d149-4763-a0bb-0d9de11b2646-0engJournal of Coastal ResearchAtribución|info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Delta evolutionriver diversionspitsand barrierbeachENSOSediment bypassing from the new human-induced lobe to the ancient lobe of the turbo delta (gulf of Urabá, southern caribbean sea)Artículo de revistahttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Textinfo:eu-repo/semantics/articlehttp://purl.org/redcol/resource_type/ARTinfo:eu-repo/semantics/acceptedVersionhttps://www.jcronline.org/doi/full/10.2112/JCOASTRES-D-17-00221.1?=Acosta, K., 2013. La econom´ıa de las aguas del r´ıo Sinu. ´ Aguaita 25, 79–114. Aga´mez, J.F. and Arrieta, R.M., 2005. Interrelaciones Entre Variables Clima´ticas y Desarrollo Erosivo en las Playas del Area Urbana ´ Municipio de Turbo, Antioquia. Medell´ın, Colombia: Universidad de Antioquia, Undergraduate thesis, 92p. Alcald´ıa Municipal de Turbo Antioquia, 2000. Plan de Ordenamiento Territorial Turbo Antioquia 2000. Turbo, Colombia: Alcald´ıa Municipal de Turbo Antioquia, 1000p. Alca´ntara-Carrio, J.; Dinkel, T.; Portz, L., and Mahiques, M.M., 2018. ´ Two new conceptual models for the formation and degradation of baymouth spits by longshore drift and fluvial discharge (Iguape, SE Brazil). Earth Surface Processes and Landforms 43(3), 695–709. Allen, G.P.; Laurier, D., and Thouvenin, J.P., 1979. Etude ´ sedimentologique du delta de la Mahakam. Paris: TOTAL, ´ Compagnies Fran¸caises des Petroles. ´ Notes et Memoires, 15, 1–156. Andrade, C., 1993. Ana´lisis de la velocidad del viento en el mar Caribe. Boletın Cient ´ ıfico CIOH, ´ 13, 33–43. 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